View allAll Photos Tagged Splash_Pool
Geysers are hot springs that episodically erupt columns of water. They occur in few places on Earth. The highest concentration of geysers anywhere is in Yellowstone’s Upper Geyser Basin (northwestern Wyoming, USA).
Big Anemone Geyser is a frequently erupting small geyser in the southern Geyser Hill Group. It is immediately adjacent to Little Anemone Geyser - together they make up “Anemone Geyser”. Big Anemone has a nearly circular basin with a central vent and lacks a well-defined border. Encircling the cream-colored to grayish, smooth geyserite-floored vent area is abundant, well-formed, closely spaced nodules of grayish geyserite (columnar geyserite & pseudocolumnar geyserite), similar in appearance to cave popcorn (coralloids). Some small biscuit-like masses of grayish geyserite are present on the northern side of the geyser, often with apical puckered structures. The geyserite biscuits are in and along a small, irregularly-shaped, eruption splash pool. The diameter of Big Anemone Geyser, as measured across its nodulose geyserite area, is about 2.5 meters. The diameter of the feature, as measured from the outer edge of its colorful, encircling microbial mats, is about 4.5 to 5 meters.
Big Anemone’s geyserite is especially well-formed and attractive. Geyserite is a friable to solid chemical sedimentary rock composed of opal (hydrous silica, a.k.a. opaline silica: SiO2•nH2O), It forms by precipitation of hydrous silica from hot spring water. Geyserite is the dominant material at & around Yellowstone hot springs and geysers (the Mammoth Hot Springs area is a major exception to this). The silica in the geyserite is ultimately derived from leaching of subsurface, late Cenozoic-aged rhyolitic rocks by superheated groundwater. Rhyolite is an abundant rock at Yellowstone.
Big Anemone Geyser has frequent, moderately low to medium-sized, splashing eruptions. Eruption durations are about half a minute long. Intervals between eruptions starts range from about 7 minutes to almost half-an-hour. Eruption activity at adjacent Little Anemone Geyser has a delaying affect on Big Anemone’s eruption frequency. Eruption cessations at Big Anemone Geyser are impressive, rapid pool drains. Most of the erupted water ends up back in its own vent. Some eruption splash water enters Little Anemone’s basin or its runoff channel.
THE SPLASH - Pool Party Camping Le Camarguais
Le 02 Juillet 2023 de 12h à 00h
Lien Event :
www.facebook.com/events/104867795969550
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THE SPLASH - Pool Party Camping Le Camarguais
Le 02 Juillet 2023 de 12h à 00h
Lien Event :
www.facebook.com/events/104867795969550
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splash pool
Pool
Aloft Nashville-Cool Springs
7109 South Springs Drive
Franklin, Tennessee (TN), 37067
United States
www.starwoodhotels.com/alofthotels/property/overview/inde...
(615) 435-8700
THE SPLASH - Pool Party Camping Le Camarguais
Le 02 Juillet 2023 de 12h à 00h
Lien Event :
www.facebook.com/events/104867795969550
Lien Page Facebook :
www.facebook.com/thexprojectevent
Lien Page Instagram :
THE SPLASH - Pool Party Camping Le Camarguais
Le 02 Juillet 2023 de 12h à 00h
Lien Event :
www.facebook.com/events/104867795969550
Lien Page Facebook :
www.facebook.com/thexprojectevent
Lien Page Instagram :
THE SPLASH - Pool Party Camping Le Camarguais
Le 02 Juillet 2023 de 12h à 00h
Lien Event :
www.facebook.com/events/104867795969550
Lien Page Facebook :
www.facebook.com/thexprojectevent
Lien Page Instagram :
splash pool
Pool
Aloft Washington National Harbor
156 Waterfront Street
National Harbor, Maryland (MD), 20745
United States
www.starwoodhotels.com/alofthotels/property/overview/inde...
301-749-9000
Private rooftop deck, with private splash pool with hot tub / Jacuzzi. Coconut Grove, Port Douglas Australia.
Geysers are hot springs that episodically erupt columns of water. They occur in few places on Earth. The highest concentration of geysers anywhere is in Yellowstone’s Upper Geyser Basin (northwestern Wyoming, USA).
Big Anemone Geyser is a frequently erupting small geyser in the southern Geyser Hill Group. It is immediately adjacent to Little Anemone Geyser - together they make up “Anemone Geyser”. Big Anemone has a nearly circular basin with a central vent and lacks a well-defined border. Encircling the cream-colored to grayish, smooth geyserite-floored vent area is abundant, well-formed, closely spaced nodules of grayish geyserite (columnar geyserite & pseudocolumnar geyserite), similar in appearance to cave popcorn (coralloids). Some small biscuit-like masses of grayish geyserite are present on the northern side of the geyser, often with apical puckered structures. The geyserite biscuits are in and along a small, irregularly-shaped, eruption splash pool. The diameter of Big Anemone Geyser, as measured across its nodulose geyserite area, is about 2.5 meters. The diameter of the feature, as measured from the outer edge of its colorful, encircling microbial mats, is about 4.5 to 5 meters.
Big Anemone’s geyserite is especially well-formed and attractive. Geyserite is a friable to solid chemical sedimentary rock composed of opal (hydrous silica, a.k.a. opaline silica: SiO2•nH2O), It forms by precipitation of hydrous silica from hot spring water. Geyserite is the dominant material at & around Yellowstone hot springs and geysers (the Mammoth Hot Springs area is a major exception to this). The silica in the geyserite is ultimately derived from leaching of subsurface, late Cenozoic-aged rhyolitic rocks by superheated groundwater. Rhyolite is an abundant rock at Yellowstone.
Big Anemone Geyser has frequent, moderately low to medium-sized, splashing eruptions. Eruption durations are about half a minute long. Intervals between eruptions starts range from about 7 minutes to almost half-an-hour. Eruption activity at adjacent Little Anemone Geyser has a delaying affect on Big Anemone’s eruption frequency. Eruption cessations at Big Anemone Geyser are impressive, rapid pool drains. Most of the erupted water ends up back in its own vent. Some eruption splash water enters Little Anemone’s basin or its runoff channel.
Splash Pool
Pool
Aloft Green Bay
465 Pilgrim Way
Green Bay, Wisconsin (WI), 54304
United States
www.starwoodhotels.com/alofthotels/property/overview/inde...
(920) 884-0800
Splash
Pool
Aloft San Antonio Airport
838 NW Loop 410
San Antonio, Texas (TX), 78216
United States
www.starwoodhotels.com/alofthotels/property/overview/inde...
info@aloftsanantonioairport.com
(210) 541-8881
THE SPLASH - Pool Party Camping Le Camarguais
Le 02 Juillet 2023 de 12h à 00h
Lien Event :
www.facebook.com/events/104867795969550
Lien Page Facebook :
www.facebook.com/thexprojectevent
Lien Page Instagram :
THE SPLASH - Pool Party Camping Le Camarguais
Le 02 Juillet 2023 de 12h à 00h
Lien Event :
www.facebook.com/events/104867795969550
Lien Page Facebook :
www.facebook.com/thexprojectevent
Lien Page Instagram :
Wet & Splash Pool Parties during Girls in Wonderland at the Sheraton Lake Buena Vista Resort in Orlando, FL.
splash pool
Pool
Aloft Chennai, OMR - IT Expressway
102 Rajiv Gandhi Salai Sholinganallur
Chennai, Tamil Nadu, 600119
India
www.starwoodhotels.com/alofthotels/property/overview/inde...
914-640-8232
Geysers are hot springs that episodically erupt columns of water. They occur in few places on Earth. The highest concentration of geysers anywhere is in Yellowstone’s Upper Geyser Basin (northwestern Wyoming, USA).
Big Anemone Geyser is a frequently erupting small geyser in the southern Geyser Hill Group. It is immediately adjacent to Little Anemone Geyser - together they make up “Anemone Geyser”. Big Anemone has a nearly circular basin with a central vent and lacks a well-defined border. Encircling the cream-colored to grayish, smooth geyserite-floored vent area is abundant, well-formed, closely spaced nodules of grayish geyserite (columnar geyserite & pseudocolumnar geyserite), similar in appearance to cave popcorn (coralloids). Some small biscuit-like masses of grayish geyserite are present on the northern side of the geyser, often with apical puckered structures. The geyserite biscuits are in and along a small, irregularly-shaped, eruption splash pool. The diameter of Big Anemone Geyser, as measured across its nodulose geyserite area, is about 2.5 meters. The diameter of the feature, as measured from the outer edge of its colorful, encircling microbial mats, is about 4.5 to 5 meters.
Big Anemone’s geyserite is especially well-formed and attractive. Geyserite is a friable to solid chemical sedimentary rock composed of opal (hydrous silica, a.k.a. opaline silica: SiO2•nH2O), It forms by precipitation of hydrous silica from hot spring water. Geyserite is the dominant material at & around Yellowstone hot springs and geysers (the Mammoth Hot Springs area is a major exception to this). The silica in the geyserite is ultimately derived from leaching of subsurface, late Cenozoic-aged rhyolitic rocks by superheated groundwater. Rhyolite is an abundant rock at Yellowstone.
Big Anemone Geyser has frequent, moderately low to medium-sized, splashing eruptions. Eruption durations are about half a minute long. Intervals between eruptions starts range from about 7 minutes to almost half-an-hour. Eruption activity at adjacent Little Anemone Geyser has a delaying affect on Big Anemone’s eruption frequency. Eruption cessations at Big Anemone Geyser are impressive, rapid pool drains. Most of the erupted water ends up back in its own vent. Some eruption splash water enters Little Anemone’s basin or its runoff channel.
Some of you know where this is, and thats how it should stay. Very secluded little cascade in the columbia gorge.... I found this first a few months ago and I took a different route this time. Its just so amazing in there. I'll be returning to this spot several more times trying different things.
THE SPLASH - Pool Party Camping Le Camarguais
Le 02 Juillet 2023 de 12h à 00h
Lien Event :
www.facebook.com/events/104867795969550
Lien Page Facebook :
www.facebook.com/thexprojectevent
Lien Page Instagram :
Beautiful New 1 Bedroom + Den Unit! South Views On Balcony. Laminate Flooring With Stainless Steel Whirlpool Appliances, With Granite Countertop. Open Concept Dining/Living Room With Walkout To Balcony. Ensuite Washer/Dryer & 1 Parking Included. Occupancy Is Immediate. Amazing Amenities Including Pool + Baby Splash Pool, Whirlpool, Sauna, Games & Party Room. Movie & Kids Play Room. Modern Gym & Much More.
No Smoking Inside Unit, $200 Key Deposit Required, No Pets Allowed, Credit Check, References, Post Dated Chqs, Rental Application Required. 1 Or 2 Year Term Available. *Approval Subject To Interview*
Beautiful New 1 Bedroom + Den Unit! South Views On Balcony. Laminate Flooring With Stainless Steel Whirlpool Appliances, With Granite Countertop. Open Concept Dining/Living Room With Walkout To Balcony. Ensuite Washer/Dryer & 1 Parking Included. Occupancy Is Immediate. Amazing Amenities Including Pool + Baby Splash Pool, Whirlpool, Sauna, Games & Party Room. Movie & Kids Play Room. Modern Gym & Much More.
No Smoking Inside Unit, $200 Key Deposit Required, No Pets Allowed, Credit Check, References, Post Dated Chqs, Rental Application Required. 1 Or 2 Year Term Available. *Approval Subject To Interview*
Geysers are hot springs that episodically erupt columns of water. They occur in few places on Earth. The highest concentration of geysers anywhere is in Yellowstone’s Upper Geyser Basin (northwestern Wyoming, USA).
Big Anemone Geyser is a frequently erupting small geyser in the southern Geyser Hill Group. It is immediately adjacent to Little Anemone Geyser - together they make up “Anemone Geyser”. Big Anemone has a nearly circular basin with a central vent and lacks a well-defined border. Encircling the cream-colored to grayish, smooth geyserite-floored vent area is abundant, well-formed, closely spaced nodules of grayish geyserite (columnar geyserite & pseudocolumnar geyserite), similar in appearance to cave popcorn (coralloids). Some small biscuit-like masses of grayish geyserite are present on the northern side of the geyser, often with apical puckered structures. The geyserite biscuits are in and along a small, irregularly-shaped, eruption splash pool. The diameter of Big Anemone Geyser, as measured across its nodulose geyserite area, is about 2.5 meters. The diameter of the feature, as measured from the outer edge of its colorful, encircling microbial mats, is about 4.5 to 5 meters.
Big Anemone’s geyserite is especially well-formed and attractive. Geyserite is a friable to solid chemical sedimentary rock composed of opal (hydrous silica, a.k.a. opaline silica: SiO2•nH2O), It forms by precipitation of hydrous silica from hot spring water. Geyserite is the dominant material at & around Yellowstone hot springs and geysers (the Mammoth Hot Springs area is a major exception to this). The silica in the geyserite is ultimately derived from leaching of subsurface, late Cenozoic-aged rhyolitic rocks by superheated groundwater. Rhyolite is an abundant rock at Yellowstone.
Big Anemone Geyser has frequent, moderately low to medium-sized, splashing eruptions. Eruption durations are about half a minute long. Intervals between eruptions starts range from about 7 minutes to almost half-an-hour. Eruption activity at adjacent Little Anemone Geyser has a delaying affect on Big Anemone’s eruption frequency. Eruption cessations at Big Anemone Geyser are impressive, rapid pool drains. Most of the erupted water ends up back in its own vent. Some eruption splash water enters Little Anemone’s basin or its runoff channel.
Splash
Pool
Aloft San Antonio Airport
838 NW Loop 410
San Antonio, Texas (TX), 78216
United States
www.starwoodhotels.com/alofthotels/property/overview/inde...
info@aloftsanantonioairport.com
(210) 541-8881
Artist: Tom Grimsey
Title: The Flowering of the Lort Burn, 2005
Material: Terrazzo, ceramic, stainless steel, planting
The Florid Burn, the Hidden Rivers Project
Leazes Park
Newcastle upon Tyne, Tyne and Wear, England, UK
Text from the Newcastle City Council web page:
The work is a direct response to the Lort Burn that flows beneath Leazes Park and through the lake. The work consists of a stream made from blue terrazzo and planting. Stainless steel flowers are set into the paths where to mark where the burn flows. A playful splash-pool, situated at the top of the park suggests the source of the Lort Burn.
Geysers are hot springs that episodically erupt columns of water. They occur in few places on Earth. The highest concentration of geysers anywhere is in Yellowstone’s Upper Geyser Basin (northwestern Wyoming, USA).
Big Anemone Geyser is a frequently erupting small geyser in the southern Geyser Hill Group. It is immediately adjacent to Little Anemone Geyser - together they make up “Anemone Geyser”. Big Anemone has a nearly circular basin with a central vent and lacks a well-defined border. Encircling the cream-colored to grayish, smooth geyserite-floored vent area is abundant, well-formed, closely spaced nodules of grayish geyserite (columnar geyserite & pseudocolumnar geyserite), similar in appearance to cave popcorn (coralloids). Some small biscuit-like masses of grayish geyserite are present on the northern side of the geyser, often with apical puckered structures. The geyserite biscuits are in and along a small, irregularly-shaped, eruption splash pool. The diameter of Big Anemone Geyser, as measured across its nodulose geyserite area, is about 2.5 meters. The diameter of the feature, as measured from the outer edge of its colorful, encircling microbial mats, is about 4.5 to 5 meters.
Big Anemone’s geyserite is especially well-formed and attractive. Geyserite is a friable to solid chemical sedimentary rock composed of opal (hydrous silica, a.k.a. opaline silica: SiO2•nH2O), It forms by precipitation of hydrous silica from hot spring water. Geyserite is the dominant material at & around Yellowstone hot springs and geysers (the Mammoth Hot Springs area is a major exception to this). The silica in the geyserite is ultimately derived from leaching of subsurface, late Cenozoic-aged rhyolitic rocks by superheated groundwater. Rhyolite is an abundant rock at Yellowstone.
Big Anemone Geyser has frequent, moderately low to medium-sized, splashing eruptions. Eruption durations are about half a minute long. Intervals between eruptions starts range from about 7 minutes to almost half-an-hour. Eruption activity at adjacent Little Anemone Geyser has a delaying affect on Big Anemone’s eruption frequency. Eruption cessations at Big Anemone Geyser are impressive, rapid pool drains. Most of the erupted water ends up back in its own vent. Some eruption splash water enters Little Anemone’s basin or its runoff channel.